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ePub Wide-Angle Seismic Reflection Profiling on Inland Waterways (IGS reports) download

by D.M. McCann,C. McCann

ePub Wide-Angle Seismic Reflection Profiling on Inland Waterways (IGS reports) download
Author:
D.M. McCann,C. McCann
ISBN13:
978-0118842280
ISBN:
0118842285
Language:
Publisher:
Stationery Office Books (December 31, 1982)
Category:
Subcategory:
Earth Sciences
ePub file:
1201 kb
Fb2 file:
1338 kb
Other formats:
lrf mobi mbr lrf
Rating:
4.2
Votes:
948

Wide Angle Seismic Re. .Wide-Angle Seismic Reflection Profiling on Inland Waterways (IGS Reports).

Wide Angle Seismic Re.See a Problem? We’d love your help. 0118842285 (ISBN13: 9780118842280).

The seismic reflection profile, which was interpreted in the light of borehole .

The seismic reflection profile, which was interpreted in the light of borehole information in the area and the results of McCann and McCann (1982), successfully identified the surface of the Palaeozoic rocks. Wide-angle upper mantle reflections were also recorded from the Lake Taupo shot; a simple T² versus X² analysis of these reflections gives a depth of about 16±1 km to the upper mantle with a root-mean-square (. velocity for the crust of . 4 ± . km/s. Commondepthpoint seismic reflection data were generated on a computer using simple ray tracing and analyzed with processing techniques currently used on actual field recordings.

However, McCann and McCann (1982) used a high-power sparker source (14 kJ) on the nearby Grand Union Canal for a wide angle seismic reflection survey and achieved a maximum penetration of 250 m, which is comparable with the results obtained on land with the seismic sources.

However, McCann and McCann (1982) used a high-power sparker source (14 kJ) on the nearby Grand Union Canal for a wide angle seismic reflection survey and achieved a maximum penetration of 250 m, which is comparable with the results obtained on land with the seismic sources mentioned above. The seismic reflection profile, which was interpreted in the light of borehole information in the area and the results of McCann and McCann (1982), successfully identified the surface of the Palaeozoic rocks

1987, Deep Seismic Reflection Profiling of the Continental Lithosphere,Geophys. CrossRefGoogle Scholar.

1987, Deep Seismic Reflection Profiling of the Continental Lithosphere,Geophys. So. Volume 89, London.

Reflection-seismic exploration became a practical tool for subsurface work and the delineation of large-scale stratigraphic architecture with the developments in seismic stratigraphy published by Vail et al. (1977). Since that time, stratigraphy itself has been revolutionized by Vail’s sequence methods. By the mid-1980s, three-dimensional seismic had become standard industry practice, and since that time, advances in acquisition technology and in computer processing power have vastly improved the ability of the technology to reveal important stratigraphic detail

Vertical Seismic Profile (VSP) is a technique of seismic measurements used for high resolution seismic imaging.

Vertical Seismic Profile (VSP) is a technique of seismic measurements used for high resolution seismic imaging. It can also be used for correlation with surface seismic data providing velocity information and information for processing such as deconvolution parameters. The defining characteristic of a VSP is that the detectors are in a borehole.

High-Resolution Seismic Reflection Profiles for the Reconstruction of Postglacial Transgressive Shorelines: An example from Greece

High-Resolution Seismic Reflection Profiles for the Reconstruction of Postglacial Transgressive Shorelines: An example from Greece.

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Reflection seismology (or seismic reflection) is a method of exploration geophysics that uses the principles of seismology to estimate the properties of the Earth's subsurface from reflected seismic waves. The method requires a controlled seismic source of energy, such as dynamite or Tovex blast, a specialized air gun or a seismic vibrator, commonly known by the trademark name Vibroseis. Reflection seismology is similar to sonar and echolocation